Iain Hartley
PhD Student at the University of York.
Supervisor: Professor Phil Ineson
Soil organic matter contains approximately twice as much carbon as the
atmosphere and soil respiration is generally the largest flux contributing
to total terrestrial ecosystem respiration. Model predictions suggest that
the potential positive feedback of soil respiration to increased
temperature will be a key factor determining the rate of global climate
change. However, the temperature sensitivities of the different component
fluxes of soil respiration may differ and rhizosphere respiration may
primarily be controlled by photosynthetic activity. The temperature
sensitivity of the decomposition of older soil organic matter is poorly
understood and is of critical importance in predicting the magnitude and
duration of any soil respiration response to global warming. With the aid
of isotopic techniques and continuous monitoring of soil respiration in the
laboratory we aim to increase our understanding of the importance of
substrate supply and quality versus temperature in determining soil
respiration rates.
Links
Contact details
Home |
Mission Statement |
CTCD Organisation |
Science Projects
A man and his spade (WARNING: soil scientist in action).
PhD topic: Carbon dynamics in forest soils - responses to global change: COMPLETED June 2006
Full details of PhD Projects
Area 2
Biology Department
University of York
Heslington
York
YO10 5DD
United Kingdom
e: iph106 at york dot ac dot uk
t: +44 (0) 1904 328594
Participating Organisations |
People |
News |
Contacts